Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction

The timing and connections between global cooling, marine redox conditions, and biotic turnover are underconstrained for the Late Ordovician. The second most severe mass extinction occurred at the end of the Ordovician period, resulting in ~85% loss of marine species between two extinction pulses. A...

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Detalles Bibliográficos
Autores principales: Kozik, Nevin P., Young, Seth A., Newby, Sean M., Liu, Mu, Chen, Daizhao, Hammarlund, Emma U., Bond, David P. G., Them, Theodore R., Owens, Jeremy D.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2022
Materias:
Earth, Environmental, Ecological, and Space Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9674285/
https://www.ncbi.nlm.nih.gov/pubmed/36399571
http://dx.doi.org/10.1126/sciadv.abn8345

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